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Magnetocrystalline and structural phase transitions of compounds MOCl (M = Ti, V, Cr, Fe) in dependence on pressure and temperature.

Subject Area Mineralogy, Petrology and Geochemistry
Term from 2017 to 2023
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 386411512
 
Final Report Year 2024

Final Report Abstract

Layered compounds MOCl (M = Ti, V, Cr, Fe) are paramagnetic at ambient conditions. Orbital order of the unpaired 3d electrons of the M3+ ions is responsible for the low-dimensional magnetic properties. The orthorhombic FeOCl structure type is frustrated for antiferromagnetic (AFM) order. Upon cooling, a spin-Peierls state develops in TiOCl (Ti3+ has a single 3d electron), and AFM order develops in VOCl, CrOCl and FeOCl. The AFM order is the result of strong magnetoelastic coupling, whereby the magnetic frustration is relieved by a monoclinic lattice distortion. Rising pressure at room temperature leads to phase transitions at a critical pressure of pc ≈ 15 GPa for all MOCl. This is a pure structural transition, without a magnetic component. For p > pc, a modulated, that is aperiodic crystal structure allows for more favorable Cl–Cl distances within the Van-der-Waals gaps between the layers MOCl, than is possible in the FeOCl structure type. In the project we have performed high-pressure (HP), lowtemperature (LT) single-crystal x-ray diffraction (SXRD) experiments on MOCl crystals. FeOCl has a phase transition from paramagnetic to monoclinic–AFM at TN = 81 K under atmospheric pressure. We have found a positive pressure coefficient ∆TN/∆p = 2.13 K/GPa, which can be explained by the pressure dependence of the crystal structure. The behavior of CrOCl is similar, but different on details, including a positive pressure coefficient of the magnetic transition temperatures. The structural transition of MOCl at room temperature and pc ≈ 15 GPa takes place within the orthorhombic paramagnetic phase. The same transition takes place at the same pc ≈ 15 GPa within the monoclinic or triclinic, AFM ordered phases at low temperatures. The monoclinic and triclinic lattice distortions are much larger at high pressure than at low temperatures and atmospheric pressure. This property could have implications for the recently manufactured, single-layer materials MOCl for spintronics, as well as for understanding of Vander-Waals heterostructures. TiOCl undergoes phase transitions to a c-axis-monoclinic, incommensurate spin-Peierls state at Tc2 = 91 K and an a-axis-monoclinic, commensurate spin-Peierls state at Tc1 = 67 K. Including literature data, a preliminary (p,T) phase diagram was constructed. Large positive pressure coefficients, ∆Tc1/∆p and ∆Tc2/∆p, are in agreement with the incommensurate transition taking place at 7 GPa at room temperature. Furthermore, we propose an unusual reentrant behavior of the incommensurate spin-Peierls phase, which forms out of the commensurate phase at temperatures below 200 K and pressures above 8 GPa. For p > pc ≈ 15 GPa, the structural modulation and the incommensurate spin-Peierls state coexist. A comprehensive analysis is presently in progress of the (p,T)-dependence of the crystal structures and possible implications for the magnetic interactions in TiOCl.

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